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an important form
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  重要形式
     Library is an important form of public knowledge space, and is different from other public knowledge spaces, such as school and museum.
     图书馆是公共知识空间的一种重要形式,它不仅承担了公共空间的永恒意义和价值,同时也与其他公共知识空间形式,如学校、博物馆等有着不同的特质。
短句来源
     Digital construction is the main direction of library construction,and the network service is an important form of the library service in the future.
     数字化建设是图书馆建设的主要方向,网络服务是未来图书馆服务的重要形式
短句来源
     Electronic commerce has gradually become an important form in the development of international trade.
     电子商务已逐渐成为国际贸易发展的重要形式
短句来源
     ESOP, regarded as employee's welfare, is an important form of supplementary pension.
     雇员持股计划(ESOP)作为雇员福利,它是企业年金的一种重要形式
短句来源
     "Seminar"is an important form of college teaching in western countries.
     "Seminar"是西方国家大学教学的重要形式
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  “an important form”译为未确定词的双语例句
     The Eco-Industry Parks (EIPs) are an important form of practicing the eco-industry.
     生态工业园区(Eco-Industrial Parks,EIPs)是生态工业的重要实践形式。
短句来源
     The inter-enterprise network has become an important form of organization that, however, the existing theories pay little attention to.
     企业间网络已经日益成为现实生活中一种重要的组织形式,但是,现有的经济理论对于这种组织形式关注很少。
短句来源
     An Important form to Realize the Acceleration of Railroad Development——Joint-stock System
     股份制是加快铁路发展的重要实现形式
短句来源
     Seen from the developing circumstances, electronic commerce will become an important form and main means for the business competition in the 21th century.
     从目前全球的发展情况看,电子商务将成为21世纪商务和贸易活动的重要形态以及企业竞争的主要手段,互联网和电子商务的兴起,将对整个社会经济生活产生巨大的影响。
短句来源
     It is an important form that current information service quality guarantee sys- tem foundation in order to heighten information service credit guarantee system construction.
     加强信息服务保障诚信机制建设,成为当前信息服务质量保障体系构建的重要组成部分。
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  相似匹配句对
     Business expansion is an important form of development.
     企业扩张是企业发展的重要形式。
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     Clustering is an important data mining form.
     聚类是一种重要的数据挖掘形式。
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     is an important vegetable.
     是一种重要的蔬菜作物。
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     An Important Breakthrough
     伟大的突破
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     On form
     “形式”论
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  an important form
Protein histidine phosphorylation is now recognized as an important form of post-translational modification.
      
In this paper, we consider an important form of electronic publication that is not frequently analyzed: the lecture, as reproduced and extended electronically.
      
Product characteristic and market modification actions were characterized as forms of regulatory intervention, while technology creation actions were characterized as an important form of federal research and development (R>amp;amp;D) intervention.
      
We also give for elements of that Pták sum an important form for their expression.
      
The pattern of body mass change suggests that the period of lactation is critical for females and endurance rivalry is an important form of competition among males.
      
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The present study is based mainly on 17 genera and 26 species of rugose coralscollected from the Lower Devonian miogeosynclinal deposits at Alengchu of Lijiang,N.W.Yunnan.10 species are considered as new and 8 indeterminable.Judgingfrom their characteristic features,five rugose coral assemblages may be preliminarilyrecognized as follows:Assemblage 1 contains Tryplasma cf.subcruciatum(Zheltonogova)and Cysticono-phyllum sp.,referring provisionally to the basal part of the Devonian.Assemblage 2 occurring in the...

The present study is based mainly on 17 genera and 26 species of rugose coralscollected from the Lower Devonian miogeosynclinal deposits at Alengchu of Lijiang,N.W.Yunnan.10 species are considered as new and 8 indeterminable.Judgingfrom their characteristic features,five rugose coral assemblages may be preliminarilyrecognized as follows:Assemblage 1 contains Tryplasma cf.subcruciatum(Zheltonogova)and Cysticono-phyllum sp.,referring provisionally to the basal part of the Devonian.Assemblage 2 occurring in the Shanjiang Formation includes Spongophyllum pseu-dofritchi(Soshkina),S.cyathophylloides(Zheltonogova),Gurjevskiella cylindricaZheltonogova,Spongphylloides?sp.and Tryplasma devoniana(Soshkina).Its assign-ment to the Upper Lochkovian age may be due to the accompanying presence of theindex Nowakiids:Paranowakia bohemica,P.intermedia,and P.obuti.Assemblage 3 known as the principal fauna in this area,occurring in the lowerpart of the Alengchu Formation.Gurjeuskiella cylindrica still persists,however,Lyrielasma chapmani Pedder seems to be an important form which together withEmbolophyllum alengchuense,Pseudochonophyllum lijiangense Constitutes the majorityof this fauna.This assemblage could be correlated approximately with those of theUpper Putonggou Formation of West Tsinling.It deserves to be mentioned thatmany species of this fauna are known to occur in the Lower Devonian Garra For-mation and its corresponding beds of southeastern Australia and some may be com-parable with those of the Malobachat beds and the Krekov beds of the Salair.Accordingly,this assemblage is considered to be Lower Praguian in age.Assemblage 4 lying in the upper part of the Alengchu Formation is found quitedistinct in component form from th Assemblage 3,exclusively of Embolophyllum whichcontinues into existence on rare occasions.Besides fewer species referring to thegenera Phacellophyllum,Fasciphyllum,this assemblage contains simple monozoniccorals:Tryplasma hercynica(Peetz),T.devoniana(Soshkina),Enterolasma stric-tum Simposon and some new species of Siphonophrentis and Aknisophyllum.Allbut Tryplasma are very common in the Lower Devonian of the eastern part of NorthAmerica.It is presumed that their similarity may be due to the convergence throughevolutionary adaptation to similar environment.On the whole,this assemblage is ofPraguian age,representing probably the later,rather than early part of the stage.Assemblage 5 present in the Banmandaodi Formatiom,consists of Tryplasma de-voniana(Soshkina),Siphonophrentis alengchuensis sp.nov.,Pseudoblothrophyllum?elegans sp.nov.and Fasciphyllum minor sp.nov.Taking into account the fact that these species appeared concurrently with the important ammonoids elements Aneto-ceras,Erbenoceras,Teicherticeras and the tentaculites Nowakia zlichovensis and N.bar-randei,it is suggested that this assemblage belongs to the Zlichovian age.Description of New SpeciesSiphonophrentis alengchuensis sp.nov.(Pl.Ⅰ,figs.1—2)It differs from Siphonophrentis giganteum(Lesueur)of the Onondaga limestone(lower to lower Middle Devonian)of N.America in having 30 majors in 16 mm.ofadult diameter and in the more or less concave tabulae.It is also distinguished fromS.variablis Oliver by the more or less complete tabulae in regular pattern and bylesser thickening of the septaPseudoblothrophyllum.elegans sp.nov.(Pl.Ⅰ,fig.7)This species assigned provisionally to genus Pseudoblothrophyullum is characteri-zed by having 30 majors in 13 mm.of adult diameter and by the incomplete and irre-gularly disposed tabulae and may be distinct from P.helderbergium Oliver of theLower Devonian in New York,U.S.A.Fasciphyllum minor sp.nov.(Pl.Ⅲ,fig.1)Corallum weakly phacelloid,with small cylindrical corallites,2.5—3.5 mm.in dia-meter,Wall 0.1 to 0.4 mm.thick.Majors numbering 14—15 and touching on in thecenter.Minors commonly rudimentary,Dissepiments large and elongate in one row(rarely two).Tabulae thinner,slightly concave.Pseudochonophyllum laticystosum sp.nov.(Pl.Ⅱ,fig.2)Up to 38 mm.in diameter.Septa wedge-shaped,38×2,periodically dilated inouter dissepimentarium,being laterally in contact with,or splitting into,two or threeparallel or anastomosing strands towards the wall;those in the tabularium withslightly axial dilation and bearing additional flanges arranged in a regular zig-zagpattern;dissepiments in 6 rows of large cystose plates being slightly inclined outward-ly and becoming steeply inclined axially,naotic structure not prominent.Tabulariumabout 1/4 to 1/5 radius.Tabulae thinner,incomplete and slightly convex.Pseudochonophyllum lijiangense sp.nov.(Pl.Ⅱ,fig.1)The main difference between the present species and the preceding one liesmainly in the shape and the inclination of the dissepiments,the former being to acertain extent numerous and smaller in size.Gurjevskiella subconica sp.nov.(Pl.Ⅱ,fig.3)It differs from G.parvulum(Strusz)of the Lower Devonian of Australia in thelarger corallum and in having 32×2 septa in 19 mm.diameter.Embolophyllum alengchuense sp.nov.(Pl.Ⅱ,fig.7)Septa wedge-shaped,28×2 septa in adult diameter of 20.7 mm.Wall essentially aseptal stereozone of variable width.Majors extending nearly to axis,arranged in abilaterally symmetrical way,slightly wavy and weakly carinate in tabularium.Minorsrestricted within dissepimentarium.Dissepiments 7 rows,commonly larger in theperiphery and becoming smaller and steeply inclined toward axis.Tabularium.mo-derately wide with sagging tabularial floors formed by incomplete and slightly con-vexed tabellae.Stereoxylodes yunnanensis sp.nov.(Pl.Ⅱ,fig.9)Solitary,up to 35 mm.septa 36×2,arranged in radially symmetrical pattern, variably thickened in outer dissepimentarium,with stout yard-arm and zigzag cari-nae.Majors extending near the centre,becoming thinner and slightly flexuous intabularium.Dissepiments small and globose in 8 to 10 rows,inclined steeply toaxis.Tabularial ca 1/3 radius.Tabulae domed axially,surrounded by small vesi-cular and peripherally iclined tabellae.Spongophyllum lijiangense sp.nov.(Pl.Ⅲ,fig.5)Cerioid,with small corallites mostly 2.5 to 3.5mm in diameter.Wall about0.1 mm.in thickness.Majors ca 10 to 12,extending almost from wall to the center,Minors variably developed or absent.Tabulae thinner,depressed axially,0.3—0.35 mm.apart.Lonsdaleoid dissepiments in one(rarely two)steeply inclined row.

本文记述云南丽江阿冷初剖面下泥盆统四射珊瑚17属26种,其中10新种,8未定种;自下而上划分出五个珊瑚组合,时代大致相当晚洛郝柯夫期至兹利柯夫期。根据珊瑚群的对比,认为丽江珊瑚群与我国西秦岭区早泥盆世四射珊瑚群比较接近,尤其是相当于布拉格期的几个组合更为密切,与澳大利亚东部,苏联萨彦—阿尔泰区同期的珊瑚群也比较接近,但是与我国南方东部地区同期的珊瑚群比较,差异则比较明显。

The through goods train originated at one loading point is an important form for organizing wagon flow in our railway transportation. In order to determime a reasonable organization form of the through goods trains, it is necessary to select a preferable organization program for them.Thus, the first step is to obtain the programs which may be comparable. The author is attempted to deal with the above-mentioned subject in this paper. This paper deals with the reasonable extent which means of forming...

The through goods train originated at one loading point is an important form for organizing wagon flow in our railway transportation. In order to determime a reasonable organization form of the through goods trains, it is necessary to select a preferable organization program for them.Thus, the first step is to obtain the programs which may be comparable. The author is attempted to deal with the above-mentioned subject in this paper. This paper deals with the reasonable extent which means of forming organization programs for the through goods trains, the destination station of operating the through goods trains, the method of forming the programs for each particular destination station of through goods trains and the method of forming the organization programs for through goods trains. It should be noted that this paper is one part of the content referred to the whole subject about the selection of the preferable organization program for through goods trains.

始发直达列车是我国铁路采用的一种重要的车流组织形式。为了确定直达列车的合理组织形式,需要选择有利的直达列车组织方案。为此,首先要得到可能参加比较的(即可比)方案。本文研究这一问题。本文研究了生成直达列车组织方案的合理范围(即装车区)、开行的直达列车到达站、各到达站直达列车方案的生成关系与方法以及直达列车组织方案的生成方法。本文是选择有利直达列车组织方案这一整个问題中的一部分内容。

Sand wave movement is an important form of sediment movement for alluvial rivers and has a great effect on stream resistance. The research of sand wave movement is of great significance to the study of sediment movement and fluvial processes and river regulation. Based on investigation and analysis of sand wave data from the flumes and rivers both abroad and at home, the formulae for the height and velocity of sand wave and the bed load rate are obtained in this paper.

沙波运动是冲积河流泥沙运动的一种重要形式。沙波的消长对河道水流的阻力损失有很大的影响。研究沙波的运动规律对研究泥沙运动、河床演变和河道整治具有十分重要的意义。本文对国内外有关水槽与天然河道实测顺行沙波资料进行了分析研究,提出了计算沙波波高及波速和推移质单宽输沙率的公式。

 
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